Results 191 to 200 of about 66,192 (275)
Water Versus Land on Temperate Rocky Planets. [PDF]
Guimond CM +8 more
europepmc +1 more source
Known unknowns, Google Earth, plate tectonics and Mt Bellenden Ker: some thoughts on locality data. [PDF]
Mesibov R.
europepmc +1 more source
Abstract Ribbon collision is a process that can rapidly disturb the symmetry of subduction zones. Previous studies have demonstrated how ribbon collision causes rotation at the surface and contortion in the slab, but have only focused on the surface kinematics.
Andres Rodriguez‐Corcho +4 more
wiley +1 more source
Plate tectonics of virus shell assembly and reorganization in phage φ8, a distant relative of mammalian reoviruses. [PDF]
El Omari K +8 more
europepmc +1 more source
Abstract The Appalachian‐Caledonian orogen was built during the Paleozoic by accretion of peri‐Gondwanan terranes onto Laurentia, culminating in the formation of Pangea. During the Mesozoic, Pangea broke apart, displacing one section of the belt to eastern North America and another to northwestern Europe.
Roberto Masis +4 more
wiley +1 more source
Large drainage systems produced half of Mars' ancient river sediment. [PDF]
Zaki AS, Goudge TA, Mohrig D.
europepmc +1 more source
Modeling Geoid and Dynamic Topography From Tomography‐Based Thermo‐Chemical Mantle Convection
Abstract Mantle convection causes the most important contribution to the geoid and dynamic topography. With mantle density inferred from high‐resolution tomography models and numerical methods solving the governing equations of viscous mantle flow, the modeled geoid can fit the observations well.
Ronghua Cui +2 more
wiley +1 more source
Intraplate deformation of Gondwana terranes and implications for the Wilson Cycle. [PDF]
Fonseca A, De Grave J.
europepmc +1 more source
Testing Volcano Deformation Models Against 3D Seismic Reflection Imagery of Ancient Intrusions
Abstract Magma intrusion often drives uplift of the overburden and free surface. Analytical modeling of such surface uplift at active volcanoes allows us to estimate intrusion geometries and positions, as well as volume and pressure changes; these insights have proven critical to forecasting volcanic unrest and eruptions. However, it is rarely possible
C. Magee, S. K. Ebmeier, J. Hickey
wiley +1 more source

